Optimisation of the indirect impedancemetry technique; a handy technique for microbial growth measurement

In the indirect impedancemetry technique, the CO₂ produced during biological activity reacts with potassium hydroxide (KOH) solution, providing negative conductance variation. In this work, this technique was optimized, on a rapid automated bacterial impedance technique (RABIT) apparatus, developed by Don Whitley Sc. Ltd (UK). The KOH concentration and volume, as well as the temperature were tested. The dynamics of CO₂ absorption and the ratio between the conductance variation and the amount of CO₂ produced were examined. After injection of CO₂ either directly in the KOH solution, or above the KOH solution, the best results were obtained with a KOH volume corresponding to immersion of the electrodes (0.7–1.2 ml), and with KOH concentrations of up to 7 g/1, although 5–6 g/l is preferred. Decrease of 280 S/mol CO₂ was obtained at 27°C for a KOH concentration ranging from 0.5 to 8 g/1. All these results were slightly affected by temperature. However, it would be preferable for the CO₂ produced to be bubbled directly into the KOH solution, in order to decrease the dynamic response of the system (gaseous transfer).     

Advancement of the cultivation and upscaling of photoautotrophic suspension cultures using <Emphasis Type="Italic">Chenopodium rubrum</Emphasis> as a case study

Photoautotrophic (PA) suspension cultures combine the advantages of cell suspensions with carbon autotrophy and have been used for various applications including studies on photosynthesis, sugar signal transduction, herbicide action, and stress responses. A major practical drawback is the requirement for elevated CO₂, which is typically generated by a buffer system in two-tier flasks that need to be custom made and require time-consuming handling. In this study, we substantially simplified and improved the cultivation of a PA culture of Chenopodium rubrum as a case study in Erlenmeyer flasks shaken in a CO₂ enriched photoincubator. Growth rates and photosynthetic activity were found to be comparable to those in two-tier flasks but with the advantage of constant CO₂ level throughout the cultivation. In addition, it was possible to establish the cultivation in a commercial laboratory-scale photobioreactor with various options to control and continuously measure the culture conditions and regimes and assess the physiological status. Although the relative biomass yield and photosynthetic performance of the batch cultures was not fully reached, the continuous cultivation system provides a good basis for future scale-up if larger amounts of biomass are needed or to impose specific cultivation regimes in combination with comprehensive online monitoring. The different improvements should contribute to the more widespread use of higher plant PA cultures and also facilitate the cultivation of microalgae.     

Exchange of oxygen between solvent H 2 O and the CO 2 produced in Cypridina bioluminescence

Bioluminescent oxidation of $\text{Cypridina}$ luciferin yields CO₂ besides oxyluciferin and light. The exchange of oxygen between the CO₂ and H₂O of the solvent becomes significant when less than approximately 1 μmol of luciferin is reacted in 4 ml of buffer solution, and the exchanged oxygen in CO₂ markedly increases by decreasing the amount of luciferin. Such an exchange is to be expected in any such system which produces CO₂ in aqueous solution, and must be taken into account in interpreting the results of experiments.     

A BATCH CULTURE METHOD FOR MICROALGAE AND CYANOBACTERIA WITH CO2 SUPPLY THROUGH POLYETHYLENE MEMBRANES1

A new method for CO₂ supply to photoautotrophic organisms was developed, and its applicability for measuring specific growth rates in shaken batch cultures of cyanobacteria and unicellular algae was shown. Small bags containing a concentrated carbonate buffer with a CO₂ partial pressure of 32 mbar were prepared from a thin foil of low density polyethylene (LDPE). These bags were inserted as CO₂ reservoirs (CRs) into polystyrene culture flasks with gas‐permeable screw caps, which were suitable to photometric growth measurement. CO₂ was released directly into the medium with membrane‐controlled kinetics. The CRs were not depleted within 1 week, although the atmosphere in the culture vessel exchanged rapidly with the ambient air. Rates of initial growth and final densities of the cultures of six different unicellular algal species and one cyanobacterium were markedly increased by diffusive CO₂ supply from the CR. In the presence of a CR, growth was exponential during the first 2 d in all cultures studied. The method described allowed a high number of measurements of specific growth rates with relatively simple experimental setup.     

Effect of Modified Atmosphere Composition on the Metabolism of Glucose by Brochothrix thermosphacta

The influence of atmosphere composition on the metabolism of Brochothrix thermosphacta was studied by analyzing the consumption of glucose and the production of ethanol, acetic and lactic acids, acetaldehyde, and diacetyl-acetoin under atmospheres containing different combinations of carbon dioxide and oxygen. When glucose was metabolized under oxygen-free atmospheres, lactic acid was one of the main end products, while under atmospheres rich in oxygen mainly acetoin-diacetyl was produced. The proportions of the total consumed glucose used for the production of acetoin (aerobic metabolism) and lactic acid (anaerobic metabolism) were used to decide whether aerobic or anaerobic metabolism predominated at a given atmosphere composition. The boundary conditions between dominantly anaerobic and aerobic metabolisms were determined by logistic regression. The metabolism of glucose by B. thermosphacta was influenced not only by the oxygen content of the atmosphere but also by the carbon dioxide content. At high CO₂ percentages, glucose metabolism remained anaerobic under greater oxygen contents.     

CO2 accumulation in bioreactor suspension cultures of Cyclamen persicum Mill. and its effect on cell growth and regeneration of somatic embryos

CO₂ accumulation in different culture systems containing embryogenic cell suspension cultures of cyclamen (Cyclamen persicum Mill.) was analyzed. In bioreactors equipped with a bubble-free or a bubble aeration system, CO₂ mole fractions in the gas phase of more than 10% were determined whereas in Erlenmeyer flasks, CO₂ mole fractions were below 2%. CO₂ accumulation in bioreactors was severely growth inhibiting in comparison to the flasks. By removing CO₂ in the aeration gas of a bubble-free aerated bioreactor, cell growth comparable to that in flasks was achieved. The regeneration ability of cell suspensions after being cultured in bioreactors with CO₂ accumulation was better than those after culture in bioreactors without CO₂ accumulation or in flasks. Received: 16 June 1998 / Revision received: 13 August 1998 / Accepted: 1 December 1998     

Atmospheric stability in cell culture vessels

Summary We have investigated the atmospheric stability in polystyrene and glass cell culture vessels by measuring the dissolved O₂ and CO₂ in the media of both seeded and unseeded culture vessels incubated at 37°C. There was no diffusion of either O₂ or CO₂ through glass vessels. At low partial pressures of oxygen (P_{O 2}), oxygen diffused into the polystyrene flasks at a rate of 1 to 2 mm Hg per 24 hr, and at high P_{O 2}, oxygen diffused slowly out of polystyrene flasks. CO₂ diffused out of polystyrene flasks with a half-time of 260 hr resulting in a considerable elevation in pH. In seeded polystyrene flasks with the P_{O 2} ⩽ room air, cellular oxygen consumption was masked by the inward diffusion of oxygen. In addition, the fall in pH due to metabolic CO₂ and organic acid production during cell growth in polystyrene flasks was buffered by the diffusion of CO₂ out of the vessels. Presented, in part, by Dr. Arthur Balin in partial fulfillment of the requirements for the Ph.D. This work was supported by USPHS grants AG-00378 from the National Institute of Aging and CA-14345 from the National Cancer Institute and NR 202-005 from the Office of Naval Research. A.K.B. is a trainee of the Medical Scientist Training Program, National Institutes of Health (GM 02046).     

TES and HEPES buffers in mammalian cell cultures and viral studies: Problem of carbon dioxide requirement

In order to evaluate TES and HEPES as a buffer system for cell culture, the proliferative capacities of cells of several mammalian cell lines in the medium buffered with either of these compounds were examined in cultures in stoppered and open flasks at high and low cell densities. When cultivated in stoppered flasks, cells grew equally well or even better in TES- and HEPES-buffered medium than in NaHCO₃-buffered medium irrespective of cell culture density. In open flasks or Petri dishes in TES- or HEPES-buffered medium, however, the proliferative capacity of cells in low density cultures was limited. The inhibition of cell growth in the latter condition was restored (1) as the cell density of the cultures increased; (2) by feeding continuously the cultures with the gas produced by high density cultures; (3) by introducing a small amount of CO₂ to the environment.These and other evidences presented suggest that, in agreement with the prevailing notions, CO₂ is required by cells as an essential nutrient for growth, and that the desired level of CO₂ in culture can be maintained efficiently by its production by even a small number of cells in culture as long as the culture flasks are stoppered. If flasks are not stoppered, however, the level of CO₂ tension is determined by an equilibrium between the rate of its production by the cells and that of escape from culture to air, resulting in the observed failure in growth of cells in TES- and HEPES-buffered medium at low cell densities unless cultures were further supplemented with added CO₂.     

Effect of carbon dioxide and ethylene on berberine production and cell browning in Thalictrum minus cell cultures

Cultured cells of Thalictrum minus L. (Ranunculaceae), transferred from culture flasks to a bubble column bioreactor, produced little berberine and turned dark brown, even when supplied with sufficient oxygen. This phenomenon was ascribed to the removal of CO₂ from the culture medium by bubbling air, and could be reproduced in flask cultures artificially deprived of CO₂. The induction of cell browning by exogenously administered ethylene suggested that CO₂ probably acts antagonistically against endogenously generated C₂H₄. The physiological damage caused by forced aeration could be prevented by adding 2 % CO₂ to the air in the bioreactor.     

The photooxidation of glyoxylate by envelope-free spinach chloroplasts and its relation to photorespiration

Large quantities of CO₂ are released within many photosynthesizing tissues in the light by the process of photorespiration. This CO₂ arises largely from the carboxylcarbon atom of glycolate, which is synthesized in chloroplasts during photosynthesis. Glyoxylate is then produced by the glycolate oxidase reaction. The glyoxylate may be directly decarboxylated to CO₂, but some investigators believe the glyoxylate must first be converted to glycine before CO₂ is released during photorespiration. Spinach chloroplasts with their envelope membranes removed in dilute buffer solution have now been shown to carry out the oxidative decarboxylation of [1-¹⁴C]glyoxylate, in the presence of light and manganous ions in an atmosphere containing oxygen, to yield 1 mole each of ¹⁴CO₂ and formate. Rates of enzymatic decarboxylation exceeding 50 μmoles of ¹⁴CO₂ mg chlorophyll⁻¹ hr⁻¹ were obtained at pH 7.6; hydrogen peroxide is probably the oxidant in the reaction. Heated chloroplasts are inactive under the standard conditions and there is an almost absolute requirement for each of the components listed above. Conditions for some other nonenzymatic decarboxylations of glyoxylate have also been described. [1-¹⁴C]Glycine is decarboxylated by the enzymatic system at only 1% of the rate of [1-¹⁴C]glyoxylate. Maize chloroplast preparations are much less active than spinach chloroplasts. The high rates of CO₂ produced by the spinach system directly from glyoxylate, as well as the need for light and oxygen, suggest that this reaction functions in photorespiration, and that CO₂ arises during photorespiration without glycine as a mandatory intermediate.     

Photosynthesis, Respiration and Post-illumination Fixation of CO2 by Corn Leaves as Influenced by Light and Oxygen Concentration

The effect of oxygen concentration on the rate of CO₂-uptake in continuous and intermittent light was studied as well as the CO₂-fixation during a short dark period after light was turned off. In addition the dark respiration and the CO₂-compensation point of attached and detached corn leaves were determined. Leaves of 4 to 22-day old plants were used as experimental material. A closed circuit system of an infrared carbon dioxide analyzer was employed to measure the rate of CO₂-exchange. It was found that in an atmosphere consisting of 100 % oxygen, there was about 50 per cent inhibition of the rate of CO₂-uptake in continuous and intermittent light compared to that in an atmosphere consisting of 21% oxygen. The same was true of the rate of CO₂-fixation in darkness during a short period after the light was turned off. Since the response to oxygen concentration of the CO₂-uptake in light and of the CO₂-fixation in darkness after the light was turned off were similar, it is concluded that the fixation of CO₂ in the short dark period represents an over- shoot of photosynthesis. The rate of dark respiration was little affected by the oxygen concentration in the ranges used in the experiments. The carbon dioxide compensation point which has been observed in leaves of 4 to 14-day old plants was not influenced by either oxygen concentration or light intensity. Since the changes in the rate of CO₂-uptake due to changes in the concentration of oxygen and light intensity had no effect on the CO₂-compensation point, it is concluded that a reabsorption of respiratory CO₂ by photosynthesis could not account for the low value of this point. These results are interpreted as a further corroboration of the statement that the leaves of corn lack the process of photorespiration and that dark respiration is inhibited in light. It was observed that the rate of the CO₂-uptake gradually increased in plants which were from 4 to 22-days old. The inhibitory effect of high concentration of oxygen on the rate of CO₂-uptake was relatively higher in old plants than in young ones.     

Biomass fast pyrolysis in a fluidized bed reactor under N2, CO2, CO, CH4 and H2 atmospheres

Biomass fast pyrolysis is one of the most promising technologies for biomass utilization. In order to increase its economic potential, pyrolysis gas is usually recycled to serve as carrier gas. In this study, biomass fast pyrolysis was carried out in a fluidized bed reactor using various main pyrolysis gas components, namely N₂, CO₂, CO, CH₄ and H₂, as carrier gases. The atmosphere effects on product yields and oil fraction compositions were investigated. Results show that CO atmosphere gave the lowest liquid yield (49.6%) compared to highest 58.7% obtained with CH₄. CO and H₂ atmospheres converted more oxygen into CO₂ and H₂O, respectively. GC/MS analysis of the liquid products shows that CO and CO₂ atmospheres produced less methoxy-containing compounds and more monofunctional phenols. The higher heating value of the obtained bio-oil under N₂ atmosphere is only 17.8 MJ/kg, while that under CO and H₂ atmospheres increased to 23.7 and 24.4 MJ/kg, respectively.     

Interaction of carbon dioxide and ethylene in overcoming thermodormancy of lettuce seeds

The combination of ethylene with CO₂ will completely overcome the thermodormancy of lettuce (Lactuca sativa L.) seeds at 35 C. This combination is effective if it is added to seeds either at the start or after several days of imbibition. The action of ethylene is dependent upon the CO₂ level present in the atmosphere surrounding the seeds. When CO₂ is trapped by KOH the ethylene effect is essentially nil.     

Internal transport of CO2 from the root‐zone to plant shoot is pH dependent

We investigated the fate of carbon dioxide (CO₂) absorbed by roots or internally produced by respiration using gas exchange and stable isotopic labeling. CO₂ efflux from detached leaves supplied with bicarbonate/CO₂ solutions was followed over six cycles. CO₂ effluxes were detected when bicarbonate solution at high pH was used, corresponding to 71–85% of the expected efflux. No CO₂ efflux was detected when CO₂ solutions at low pH were used but CO₂ efflux was subsequently detected as soon as bicarbonate solutions at high pH were supplied. By sealing the leaf and petiole in a plastic bag to reduce diffusion to the atmosphere, a small CO₂ efflux signal (14–30% of the expected efflux) was detected suggesting that CO₂ in the xylem stream can readily escape to the atmosphere before reaching the leaf. When the root‐zones of intact plants were exposed to CO₂ solutions, a significant efflux from leaf surface was observed (13% of the expected efflux). However, no signal was detected when roots were exposed to a high pH bicarbonate solution. Isotopic tracer experiments confirmed that CO₂ supplied to the root‐zone was transported through the plant and was readily lost to the atmosphere. However, little ¹³C moved to the shoot when roots were exposed to bicarbonate solutions at pH 8, suggesting that bicarbonate does not pass into the xylem.     

Diversity in gas exchange and muscular activity patterns in insects studied by a respirometer-actograph

Different events in insect gas exchange and muscular activity are described by a new system of automatic respirometers, a differential electrolytic microrespirometer-actograph. This is very sensitive to volumetric changes caused by insect respiration and/or body movements. In this system, oxygen generation and its regulation are combined in the same current circuit. According to this principle, the oxygen consumed by the insect is continuously replaced by equal amounts of electrolytically produced oxygen. This simple laboratory-made apparatus records simultaneously metabolic rate, the cyclicity of external gas exchange, rhythms of muscular ventilating and the pattern of other body movements, including abdominal pulsations not observable with the naked eye. The respirometer-actograph described here is applicable also to the recording of the respiration of other terrestrial arthropods or other living organisms or tissues.     

Gas composition strategies for the successful scale-up of Catharanthus roseus cell cultures for the production of ajmalicine

Ajmalicine, serpentine, catharanthine, and vindoline are monoterpenoid indole alkaloids (MIAs) of commercial interest which are produced by the Catharanthus roseus plant. Cultures of C. roseus have been investigated as a potential source of these pharmaceutically important compounds since the early 1960s. In addition, their production from C. roseus cultures has served as a model system for investigating secondary metabolism and for evaluating production-enhancing strategies. Initially, this review will survey (1) the MIAs of interest for large-scale production from plant cell cultures and (2) the volumetric productivities of a specific MIA, ajmalicine, achieved and projected using plant cell cultures. To meet the need for these valuable compounds, the production of these MIAs from plant cell cultures must be successfully reproduced in large-scale aerated and agitated reactors. While the large-scale cultivation of plant cell cultures is currently feasible, initial attempts at scale-up may yield results that differ from that optimized in flasks. To bridge the jump between production in flasks and production in large-scale bioreactors, changes introduced with scale-up such as gas composition must be identified and rationally manipulated to reproduce or even improve growth and secondary metabolite production. Hence, this review will (1) identify the effects of gas composition (i.e., O₂, CO₂, ethylene, or other endogenous volatile compounds) on growth and secondary metabolism and (2) draw operating strategies for optimizing the gas composition for growth of C. roseus cultures and the production of ajmalicine.     

Batch culture of bacteria under controlled gaseous conditions

Summary A flask, designed for direct gassing of batch cultures of bacteria, was evaluated for its use in studying oxygen absorption rates (OAR) and suitability for physiological studies under various controlled atmospheres. Such flasks, aerated directly without shaking, yielded an OAR (up to 1.2 mmol O₂/l/min) that was comparable to or higher than those obtained in conventional flasks aerated by shaking. Direct aeration in combination with shaking resulted in OAR values that were elevated and most favorable for growth of oxygen demanding bacteria (5 mmol O₂/l/min). In comparison with controls, the direct method of aeration in combination with shaking proved most efficient and least dependent on the surface to volume ratio of the aerated solution. In experiments with the facultative anaerobe Streptococcus faecalis 10Cl, grown in controlled aerobic, anaerobic, and mixed gas (CO₂-free air, air-plus-CO₂, N₂-plus-CO₂) environments, a specific anaerobic requirement for CO₂ could be established. The wide range of gaseous environments possible renders the newly tested flask useful for comparative biochemical studies, especially when the gaseous condition of culture is a factor of critical importance.     

Proliferative and secretory activity of human umbilical endothelial cells cultivated under various hypoxia conditions

In this study, we examined the impact of 3-day hypoxia of different degrees on the viability, proliferation, and secretory activity of endothelial cells from human umbilical vein (HUVEC). A gas mixture of three components was used (%): 1) 10 O₂, 5 CO₂, and 85 Ar; 2) 5 O₂, 5 CO₂, and 80 Ar; and 3) 1 O₂, 5 CO₂, and 94 Ar. Cells cultivated in a CO₂ incubator in atmospheric oxygen (21% O₂) served as control. It was found that 3-day HUVEC cultivation at 1% O₂ increased NO synthesis; enhanced secretion of endothelin-1, IL-6, IL-8, TNF-alpha, sVCAM-1, sE-cadherin, sE-selectin, VEGF-A, and bFGF; and inhibited proliferation. HUVEC cultivated under 10% O₂ and 5% O₂ exhibited the lowest level of basal secretion of these substances and increased proliferative activity. These cells cultivated under conditions of atmospheric oxygen for 3 days displayed activated secretion of NO, IL-6, IL-8, and von Willebrand factor; the activation was higher than at 10% O₂ and 5% CO₂. Thus, the gaseous medium with reduced oxygen content (5%) is a more physiological condition for HUVEC cultivation. An increase in the amount of oxygen up to the atmospheric level causes endotheliocyte activation; the cells exhibit the features of endothelial dysfunction. Oxygen content reduced to 1% induces endothelial dysfunction and reduced proliferative potential.     

Land plants equilibrate O2 and CO2 concentrations in the atmosphere

The role of land plants in establishing our present day atmosphere is analysed. Before the evolution of land plants, photosynthesis by marine and fresh water organisms was not intensive enough to deplete CO₂ from the atmosphere, the concentration of which was more than the order of magnitude higher than present. With the appearance of land plants, the exudation of organic acids by roots, following respiratory and photorespiratory metabolism, led to phosphate weathering from rocks thus increasing aquatic productivity. Weathering also replaced silicates by carbonates, thus decreasing the atmospheric CO₂ concentration. As a result of both intensive photosynthesis and weathering, CO₂ was depleted from the atmosphere down to low values approaching the compensation point of land plants. During the same time period, the atmospheric O₂ concentration increased to maximum levels about 300 million years ago (Permo-Carboniferous boundary), establishing an O₂/CO₂ ratio above 1000. At this point, land plant productivity and weathering strongly decreased, exerting negative feedback on aquatic productivity. Increased CO₂ concentrations were triggered by asteroid impacts and volcanic activity and in the Mesozoic era could be related to the gymnosperm flora with lower metabolic and weathering rates. A high O₂/CO₂ ratio is metabolically linked to the formation of citrate and oxalate, the main factors causing weathering, and to the production of reactive oxygen species, which triggered mutations and stimulated the evolution of land plants. The development of angiosperms resulted in a decrease in CO₂ concentration during the Cenozoic era, which finally led to the glacial-interglacial oscillations in the Pleistocene epoch. Photorespiration, the rate of which is directly related to the O₂/CO₂ ratio, due to the dual function of Rubisco, may be an important mechanism in maintaining the limits of O₂ and CO₂ concentrations by restricting land plant productivity and weathering.     

Oceanic sinks for atmospheric CO2

There is approximately 50 times more inorganic carbon in the global ocean than in the atmosphere. On time scales of decades to millions of years, the interaction between these two geophysical fluids determines atmospheric CO₂ levels. During glacial periods, for example, the ocean serves as the major sink for atmospheric CO₂, while during glacial–interglacial transitions, it is a source of CO₂ to the atmosphere. The mechanisms responsible for determining the sign of the net exchange of CO₂ between the ocean and the atmosphere remain unresolved. There is evidence that during glacial periods, phytoplankton primary productivity increased, leading to an enhanced sedimentation of particulate organic carbon into the ocean interior. The stimulation of primary production in glacial episodes can be correlated with increased inputs of nutrients limiting productivity, especially aeolian iron. Iron directly enhances primary production in high nutrient (nitrate and phosphate) regions of the ocean, of which the Southern Ocean is the most important. This trace element can also enhance nitrogen fixation, and thereby indirectly stimulate primary production throughout the low nutrient regions of the central ocean basins. While the export flux of organic carbon to the ocean interior was enhanced during glacial periods, this process does not fully account for the sequestration of atmospheric CO₂. Heterotrophic oxidation of the newly formed organic carbon, forming weak acids, would have hydrolyzed CaCO₃ in the sediments, increasing thereby oceanic alkalinity which, in turn, would have promoted the drawdown of atmospheric CO₂. This latter mechanism is consistent with the stable carbon isotope pattern derived from air trapped in ice cores. The oceans have also played a major role as a sink for up to 30% of the anthropogenic CO₂ produced during the industrial revolution. In large part this is due to CO₂ solution in the surface ocean; however, some, poorly quantified fraction is a result of increased new production due to anthropogenic inputs of combined N, P and Fe. Based on ‘circulation as usual’, models predict that future anthropogenic CO₂ inputs to the atmosphere will, in part, continue to be sequestered in the ocean. Human intervention (large-scale Fe fertilization; direct CO₂ burial in the deep ocean) could increase carbon sequestration in the oceans, but could also result in unpredicted environmental perturbations. Changes in the oceanic thermohaline circulation as a result of global climate change would greatly alter the predictions of C sequestration that are possible on a ‘circulation as usual’ basis.